Abstract:Subduction of oceanic lithosphere is widely invoked for the Neoarchean but the thermal and geometrical configurations of the inferred subduction zones remain poorly constrained. Two Neoarchean subduction-related tectonic belts (A and B) with contrasting lithotectonic evolutions are preserved in the North China Craton. In Belt A, the oxygen fugacity of ca. 2.6-2.5 Ga modified mantle from crustal recycling-related basalts is coincident with modern arc mantle, but that of Belt B is more reducing. Based on the rel… Show more
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